The Encyclopaedia Britannica: A Dictionary of Arts, Sciences, and General Literature, 6. kötetThomas Spencer Baynes C. Scribner's Sons, 1878 |
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1. oldal
... temperature of about 76 ° Fabr . The population of Clifton in 1712 , the date of the second edition of Sir Thomas Alleyne's work on Gloucester , was only 450 ; in 1841 it amounted to 14,177 ; in 1857 to 17,634 ; in 1861 to 21,375 ; and ...
... temperature of about 76 ° Fabr . The population of Clifton in 1712 , the date of the second edition of Sir Thomas Alleyne's work on Gloucester , was only 450 ; in 1841 it amounted to 14,177 ; in 1857 to 17,634 ; in 1861 to 21,375 ; and ...
2. oldal
... temperature over the globe , from the great heat of equatorial regions , falling by easy gradations with increase of latitude , to the extreme cold of the poles . If the earth's surface were uniform , and its atmosphere motionless ...
... temperature over the globe , from the great heat of equatorial regions , falling by easy gradations with increase of latitude , to the extreme cold of the poles . If the earth's surface were uniform , and its atmosphere motionless ...
3. oldal
... temperature of different hours of the day at different heights , for an explanation of which we must look to the physical configuration of the earth's surface and to the nature of that surface , whether rock , sand , black soil , or ...
... temperature of different hours of the day at different heights , for an explanation of which we must look to the physical configuration of the earth's surface and to the nature of that surface , whether rock , sand , black soil , or ...
4. oldal
... temperature of sandy deserts often rises to 120 ° , 140 ° , or even to 200 ° , and the shade temperature has been observed as high as 125 ° . It is this hot air , loaded with particles of sand still notter , and driven onwards by ...
... temperature of sandy deserts often rises to 120 ° , 140 ° , or even to 200 ° , and the shade temperature has been observed as high as 125 ° . It is this hot air , loaded with particles of sand still notter , and driven onwards by ...
5. oldal
... temperature of the locality . | From this follow two important consequences , viz .- ( 1 ) during each winter no inconsiderable portion of the cold produced by terrestrial radiation is conveyed away from the surface to the depths of the ...
... temperature of the locality . | From this follow two important consequences , viz .- ( 1 ) during each winter no inconsiderable portion of the cold produced by terrestrial radiation is conveyed away from the surface to the depths of the ...
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